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Abstract
This paper challenges the existing diffuse-strain model of the Africa-Eurasia collision in the western Mediterranean by analyzing two active offshore fault systems: the Yusuf Fault System (YFS) and the Alboran Ridge Fault System (ARFS). Using seismic images, the authors estimate significant Plio-Holocene slip (16 ± 4.7 km for ARFS and a minimum of 12 km for YFS), suggesting a well-defined narrow plate boundary capable of generating significant seismic and tsunami hazards.
Publisher
Nature Communications
Published On
Aug 15, 2022
Authors
Laura Gómez de la Peña, César R. Ranero, Eulàlia Gràcia, Guillermo Booth-Rea, José Miguel Azañón, Umberta Tinivella, Abdelkarim Yelles-Chaouche
Tags
Yusuf Fault System
Alboran Ridge Fault System
Plio-Holocene slip
seismic hazards
tsunami risks
Africa-Eurasia collision
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